// lecture 19 Flashcards
pacific decadal oscillation
related to ENSO, but lower frequency and more concentrated in the middle latitudes.
impacts of the PDO:
- affects US winter weather in the same way ENSO does. for example, a negative PDO encourages drought in California.
- affects salmon abundance on the west coast because of its influence on the ocean.
- affects the global mean temp. when in its cold phase, the cold SST in the tropics can lower the global mean temp. because the ocean stores more heat and cools the atmosphere. by transition from cold to warm during 2015 El Nino caused global warming to accelerate after long period of very slow warming.
atlantic multi-decadal oscillation (AMO)
average SST over north atlantic, subtract linear trend. warm SST in tropical atlantic makes more and bigger hurricanes, all else being equal.
impacts of AMO:
- arctic seems to be warmed by warming of North Atlantic Ocean.
- hurricanes in Atlantic respond to local warming of subtropical atlantic ocean.
- PDO and AMO are low frequency (decade time scales) natural variability that can be confused with, but also interact with, global warming.
profile of tropical cyclone
- eye - clear area in the center.
- eyewall - clouds immediately surrounding the eye (highest winds and rain).
- spiral rain bands - outer raining areas.
- rising areas have rain and clouds; sinking areas are dry.
hurricanes occur over the
warmest waters, but not right at the equator because the coriolis force is required.
saffir-simpson hurricane scale
higher category = higher winds = more storm surge = lower pressure in the eye.
category 1 (ss hurricane scale)
74 mph, 980+ mbars; minimal
category 2
96 mph, 979 mbars; moderate
category 3
111 mph, 964 mbars; extensive
category 4
121 mph, 944 mbars; extreme
category 5
156+ mph, <920 mbars; catastrophic
many strong hurricanes are around
Taiwan, Philippines.
tropical cyclone Yasi
155 mph winds, 930 mbar min. pressure. among top ten strongest cyclones to hit australia soil is already saturated from floods. la nina (extremely warm ocean in w. pacific)
water vapor
fuels a hurricane. when water vapor condenses, heat is released.
heat released from a hurricane:
- 1.5 cm/day of average rainfall in a circle of radius 660 km.
- the heat released from this condensation is 52 quintrillion joules per day of energy.
- 200 times the world electricity generating capacity.
condensation is the ____ and evaporation provides the ____
energy source; fuel. the strong winds in hurricanes causes more evaporation from the ocean surface.
warmer air can hold more
moisture. also evaporation can occur more easily from a warmer ocean.
warm ocean temps.:
first requirement for hurricanes. hurricanes weaken when they pass over land due to lack of evaporation.
requirements for hurricanes
- SSTs must be above 26 C (79 F). this will shift to a warmer temp. threshold in a warmer climate though.
- must be a least 5 degrees off the equator. Coriolis force is required (why storms rotate opposite in N. and S. hemispheres).
- not much wind sheer (when the winds change with height). this rips hurricanes apart.
- can’t be too cold below the surface either.
when hurricanes pass by, they
churn up colder water from below.
damages in hurricanes are caused by:
winds, storm surge (high winds pushing towards the land), and flooding.
financial damages from hurricanes is
increasing, but this is primarily due to more people living on the coast.
1991 Bangladesh cyclone
144,000 fatalities. left 10 million homeless.